
The Gegham mountains (or Gegham Ridge; ) are a
range of mountains in
Armenia
Armenia, officially the Republic of Armenia, is a landlocked country in the Armenian Highlands of West Asia. It is a part of the Caucasus region and is bordered by Turkey to the west, Georgia (country), Georgia to the north and Azerbaijan to ...
. The range is a
tableland-type watershed basin of
Sevan Lake from east, inflows of rivers
Araks and
Hrazdan
Hrazdan ( ) is a town and urban municipal community in Armenia serving as the administrative centre of Kotayk Province, located northeast of the capital Yerevan. As of the 2011 census, the population of the town is 44,231.
During the Soviet Uni ...
from north and west, Azat and Vedi rivers from south-west and Arpachai river from south. The average elevation of the Gegham mountain range is near 2500m. The range is of volcanic origin including many
extinct volcano
A volcano is commonly defined as a vent or fissure in the Crust (geology), crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and volcanic gas, gases to escape from a magma chamber below the surface.
On Earth ...
es. The range is 70 km length and 48 km width, and stretch between
Lake Sevan
Lake Sevan () is the largest body of water in both Armenia and the Caucasus region. It is one of the largest freshwater Alpine lake, high-altitude (alpine) lakes in Eurasia. The lake is situated in Gegharkunik Province, at an altitude of abov ...
and the
Ararat plain. The highest peak of the Gegham mountains is the
Azhdahak, at 3597m. They are formed by a
volcanic field
A volcanic field is an area of Earth's Earth's crust, crust that is prone to localized volcano, volcanic activity. The type and number of volcanoes required to be called a "field" is not well-defined. Volcanic fields usually consist of clusters ...
, containing
Pleistocene
The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was fin ...
-to-
Holocene
The Holocene () is the current geologic time scale, geological epoch, beginning approximately 11,700 years ago. It follows the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene to ...
lava dome
In volcanology, a lava dome is a circular, mound-shaped protrusion resulting from the slow extrusion of viscous lava from a volcano. Dome-building eruptions are common, particularly in convergent plate boundary settings. Around 6% of eruptions ...
s and
cinder cone
A cinder cone or scoria cone is a steep, volcanic cone, conical landform of loose pyroclastic rock, pyroclastic fragments, such as volcanic ash, clinkers, or scoria that has been built around a volcanic vent. The pyroclastic fragments are forme ...
s. The highland reaches a height of 1800–2000m up to 3000m in the dividing ridge.
Geological history

Volcanism in Armenia and in the Gegham mountains is related to mantle processes accompanying, but not necessarily related to the collision of the
Arabian Plate with the
Eurasian Plate. Unlike in other parts of the
Caucasus
The Caucasus () or Caucasia (), is a region spanning Eastern Europe and Western Asia. It is situated between the Black Sea and the Caspian Sea, comprising parts of Southern Russia, Georgia, Armenia, and Azerbaijan. The Caucasus Mountains, i ...
region, the Gegham mountains have generated primarily small scale volcanoes. The Kaputan Formation (including Mt. Atis and Gtsain Ridge) from the
Late Miocene
The Late Miocene (also known as Upper Miocene) is a sub-epoch of the Miocene epoch (geology), Epoch made up of two faunal stage, stages. The Tortonian and Messinian stages comprise the Late Miocene sub-epoch, which lasted from 11.63 Ma (million ye ...
has been dated at 5.7–4.6 Ma by
K-Ar and is the oldest sequence in the region.
Late Pliocene
Late or LATE may refer to:
Everyday usage
* Tardy, or late, not being on time
* Late (or the late) may refer to a person who is dead
Music
* Late (The 77s album), ''Late'' (The 77s album), 2000
* Late (Alvin Batiste album), 1993
* Late!, a pseudo ...
activity involved various
basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial ...
ic lavas (including Lchain Volcano) and subsequently, during the
Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS), as well as the current and most recent of the twelve periods of the ...
,
rhyolite
Rhyolite ( ) is the most silica-rich of volcanic rocks. It is generally glassy or fine-grained (aphanitic) in texture (geology), texture, but may be porphyritic, containing larger mineral crystals (phenocrysts) in an otherwise fine-grained matri ...
and
obsidian
Obsidian ( ) is a naturally occurring volcanic glass formed when lava extrusive rock, extruded from a volcano cools rapidly with minimal crystal growth. It is an igneous rock. Produced from felsic lava, obsidian is rich in the lighter element ...
from the Kotayk centre (Gutansar and Atis 700 ka, then associated fissure volcanoes 550–480 ka). The volcanic activity peaked round 200 ka, when most of the Gegham centres formed from
trachyandesitic lavas. Aknotsasar and Sevkatar were active less than 100ka ago.
The highest point is the volcano
Azhdahak, elevation - 3597.3m above sea level, in the western part of the range. There is a lake in the crater of the volcano Azhdahak that is formed from melting snow.
The volcanoes Spitaksar (3560 m) and Geghasar (3446 m), the former erupted 120ka ago and the latter 80-40ka, are sources of obsidian in Armenia.
Ecology
Bird fauna of Gegham mountains includes about 250 species, 70% of all Armenia's avifauna.
The southeastern slopes of Gegham mountains contain the
Khosrov Forest, planted in the 4th century by
Khosrov I and converted into a state park in 1958.
The Gegham mountains are one of the primary presences of the
vavilovia (''Lathyrus formosus'') around Mount Sevsar. Another species ''
Poa greuteri'' is endemic in the area.
Rock carvings

A great number of
petroglyph
A petroglyph is an image created by removing part of a rock surface by incising, picking, carving, or abrading, as a form of rock art. Outside North America, scholars often use terms such as "carving", "engraving", or other descriptions ...
s - rock-carvings has been found in the area of Gegham Mountains. Most images depict men in scenes of hunting and fighting, and astronomical bodies and phenomena: the Sun, the Moon, constellations, the stellar sky, lightning, etc. Carvings of birds have attracted some archeological interest.
Gallery
File:Gegham Mountains 1.jpg
File:Gegham Mountains 4.jpg
File:Geghama mountains from Tar mount - panoramio.jpg
File:Geghama range Emma YSU (5).jpg
File:Geghama range Emma YSU (7).jpg
File:Geghama range Emma YSU (8).jpg
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Armaghan">
File:Armaghan 02.jpg
File:Armaghan mount crater (2829m).JPG
Azhdahak">
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File:-Աժդահակ S-N 05.jpg
File:.Աժդահակ 01.jpg
File:.Աժդահակ 02.jpg
Gutanasar">
File:Gutanasar, Alpian Fields 007.jpg
File:Gutanasar, Alpian Fields 008.jpg
File:Gutanasar, Alpian Fields 003.jpg
File:Gutanasar, Alpian Fields 004.jpg
File:Gutanasar, Alpian Fields 005.jpg
File:Gutanasar.jpg
File:Mount Gutanasar 01.jpg
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File:.Գեղասար 03.jpg
File:.Գեղասար 06.jpg
File:.Գեղասար 07.jpg
File:.Գեղասար 08.jpg
File:.Գեղասար 13.jpg
File:.Գեղասար 16.jpg
Lusnalich">
File:Lusnalidj 01.jpg
File:Lusnalidj 06.jpg
File:Lusnalidj 02.jpg
Menaksar">
File:Menaksar.jpg
File:Phamb pass, view from top of mount Menaksar.jpg
Sevkatar">
File:Sevkatar (Sevsar).jpg
File:Սևկատար 3225մ.jpg
Spitakasar">
File:-Ducks lakes S-N 01.jpg
File:-Ducks lakes S-N 03.jpg
File:-Ducks lakes S-N 04.jpg
File:-Mets Spitakasar S-N 01.jpg
File:Mount Phoqr Spitakasar from Mt. Spiakasar, 2013.06.23 - panoramio.jpg
File:Mount Spitakasar, 2013.06.23.jpg
References
Sources
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External links
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{{Authority control
Volcanic fields
Quaternary lava domes
Cinder cones
Mountain ranges of Armenia
Lava domes